The limited influence of glaciations in Tibet on global climate over the past 170 000 yr
- 1 January 2002
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 194 (3-4) , 287-297
- https://doi.org/10.1016/s0012-821x(01)00573-8
Abstract
No abstract availableKeywords
This publication has 36 references indexed in Scilit:
- Cosmic ray labeling of erosion surfaces: in situ nuclide production rates and erosion modelsPublished by Elsevier ,2002
- The 21Ne production rate in quartz revisitedEarth and Planetary Science Letters, 2000
- Entrainment at cold glacier bedsGeology, 2000
- The role of the heat source of the Tibetan Plateau in the general circulationArchiv für Meteorologie, Geophysik und Bioklimatologie Serie A, 1998
- Asian provenance of glacial dust (stage 2) in the Greenland Ice Sheet Project 2 Ice Core, Summit, GreenlandJournal of Geophysical Research: Oceans, 1997
- Erosion rates of alpine bedrock summit surfaces deduced from in situ 10Be and 26AlEarth and Planetary Science Letters, 1997
- Sea-Surface Temperatures and the History of Monsoon Upwelling in the Northwest Arabian Sea during the Last 500,000 YearsQuaternary Research, 1995
- Mass spectrometric identification of cosmic-ray-produced neon in terrestrial rocks with multiple neon componentsEarth and Planetary Science Letters, 1993
- Cosmogenic neon in ultramafic nodules from Asia and in quartzite from AntarcticaEarth and Planetary Science Letters, 1991
- Relative dating of Quaternary moraines, Rongbuk valley, Mount Everest, Tibet: Implications for an ice sheet on the Tibetan PlateauQuaternary Research, 1991